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Usage of Obsidian (Igneous Energy) in Both Radiation Detection and Fixed-Target Machine in Discovery of Subatomic Particles

Year 2020, Volume: 3 Issue: 1, 6 - 9, 30.06.2020

Abstract

Obsidian is amorphous
material which contains SiO2 compound and also is to be taken out
from volcanic mountains. 75% of obsidian comprises quartz. Quartz is the required
material to observe the piezoelectric effect. Obsidian originally comes from the mantle of the earth crust. When it
contacts with oxygen in the air, it solidifies suddenly with no any opportunity
that switches to crystallized state. Because of that reason, it becomes
amorphous silica. If some chemicals such as fluorine or hydrogen with respect
to semiconductors process is connected into silicon (a-si:H) that let to see
photoconductivity property will be revealed. Radiation detectors have an
ability of absorption. In this article, obsidian is debated on whether it can
be useful for radiation detection as an absorber or not and furthermore, is
evaluated if obsidian is focused on the fixed target machine as stationary
target area related with the discovery of subatomic particles.

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References

  • İpekoğlu, B.,; “Kuvars, Kuvarsit, Kuvars Kumu”, İstanbul Maden İhracatçıları Birliği, Türkiye Endüstriyel Mineraller Envanteri, (1999), 102- 106 pages
  • Ruud E.I. Schropp, M.Zeman, “Amorphous and Microcrystalline Silicon Solar Cells: Modeling, Materials and Device Technology”, Kluver Akademik Yayınevi, Boston (1998).
  • Cengiz G.; Caglar I.; Bılır G.,Optical Properties and Natural Radioactivity Levels of Turkish Natural Obsidians,Vol 6,(2019), pages 138-141.
  • Chataigner, C.; Işıklı, M.; Gratuze, B.; Çil, V.; Obsidian Sources in the Regions of Erzurum and Kars (North-East Turkey): New Data. Archaeometry 56(3), (2014), 351-374 pages.
  • Guo S. L.; Chan B. L.; Durrani S. A, Chapter 4 - Solid-State Nuclear Track Detectors, Handbook of Radioactivity Analysis (Third Edition) (2012), Pages 233-298 pages.
  • Bhagwat A. M., Solid State Nuclear Track Detection: Theory and Applications, Indian Society for Radiation Physics, (1993), 1-34 pages.
  • SiJk, E.C.H. and Barnes, R.S., Examination of fission fragment tracks with an electron microscope, Phil. Mag. 4, (1959) 970- 972 pages.
  • Fleischer RL, Price PB, Walker RM: The Ion Explosion Spike Mechanism for Formation of Charged Particle Tracks in Solids. J Appl Phys, 36:,(1965), 3645-3652 pages.
  • Roberts JH, Gold R, Armani RJ: Spontaneous Fission decay Constant of 238U. Phys Rev, (1968),1482-1484 pages.
  • Flerov GN, Perelygin VP, Otgonsuren O, On the origin of Tracks of Fission Fragments in Lead Glasses. At Energ, (1972), 33:979- 984 pages.
  • Durrani SA, Khan HA: Annealing of Fission Tracks in Tektites: Corrected Ages of Bediasites, Earth Plant Sci Lett, (1972), 9:431- 445 pages.
  • Campero AM, Fleischer RL, Likes RS: Changes in Subsurface Radon Concentration Associated with Earthquakes. Jr Geophysical res,(1980), 85: 3053-3057 pages.
  • Faul H, Wagner GA: Fission Track Dating, in Dating Techniques for the Archaeologist HN Michael and EK Ralph (eds), Cambridge: MIT Press, (1971), 152- 156 pages.
  • Macdougall JM: Meteoritics,(1975), 10:449 pages.
  • Bodu R, Bouzigues H, Morin N, Pfiffelman JP: On the Existence of Amomalous Isotopic Abundances in Uranium from Gabon. Compt rend Paris, (1972), 275:1731-1732 pages.
  • Hansen P, Heitmann H, Smit PH: Nuclear Tracks in Iron Granet Films. Phys Rev, (1982), B26:3539 pages.
  • Khan HA, Brandt R, Hirdes D, Tress G, Dersch G, Jamil K: Use of Mica Nuclear Filter in the development of a Background Free Radon Presonnel Dosimeter. Journal of Aerosol Science, (1983), 14:232-237 pages.
  • Poulsen H. P., Neuefeind J., Neumann H. B., Schneider J. R., Zeidler M. D., Amorphous silica studied by high energy X-ray diffraction, Journal of non- crystalline solids 188(1,2), (1995), 63-74 pages.
  • Martin, B.R.; Shaw G.; Particle Physics 3 rd Edition ISBN 978-0-470-03293-0.(cloth),ISBN 978-0-470-03294-7(Pbk.),(2008).
  • Heuser J.M.; Ivanov V.V., The Compressed Baryonic Matter experiment at FAIR: physics of strangeness and charm, status of preparations, In Journal of Physics G Nuclear and Particle
Year 2020, Volume: 3 Issue: 1, 6 - 9, 30.06.2020

Abstract

Project Number

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References

  • İpekoğlu, B.,; “Kuvars, Kuvarsit, Kuvars Kumu”, İstanbul Maden İhracatçıları Birliği, Türkiye Endüstriyel Mineraller Envanteri, (1999), 102- 106 pages
  • Ruud E.I. Schropp, M.Zeman, “Amorphous and Microcrystalline Silicon Solar Cells: Modeling, Materials and Device Technology”, Kluver Akademik Yayınevi, Boston (1998).
  • Cengiz G.; Caglar I.; Bılır G.,Optical Properties and Natural Radioactivity Levels of Turkish Natural Obsidians,Vol 6,(2019), pages 138-141.
  • Chataigner, C.; Işıklı, M.; Gratuze, B.; Çil, V.; Obsidian Sources in the Regions of Erzurum and Kars (North-East Turkey): New Data. Archaeometry 56(3), (2014), 351-374 pages.
  • Guo S. L.; Chan B. L.; Durrani S. A, Chapter 4 - Solid-State Nuclear Track Detectors, Handbook of Radioactivity Analysis (Third Edition) (2012), Pages 233-298 pages.
  • Bhagwat A. M., Solid State Nuclear Track Detection: Theory and Applications, Indian Society for Radiation Physics, (1993), 1-34 pages.
  • SiJk, E.C.H. and Barnes, R.S., Examination of fission fragment tracks with an electron microscope, Phil. Mag. 4, (1959) 970- 972 pages.
  • Fleischer RL, Price PB, Walker RM: The Ion Explosion Spike Mechanism for Formation of Charged Particle Tracks in Solids. J Appl Phys, 36:,(1965), 3645-3652 pages.
  • Roberts JH, Gold R, Armani RJ: Spontaneous Fission decay Constant of 238U. Phys Rev, (1968),1482-1484 pages.
  • Flerov GN, Perelygin VP, Otgonsuren O, On the origin of Tracks of Fission Fragments in Lead Glasses. At Energ, (1972), 33:979- 984 pages.
  • Durrani SA, Khan HA: Annealing of Fission Tracks in Tektites: Corrected Ages of Bediasites, Earth Plant Sci Lett, (1972), 9:431- 445 pages.
  • Campero AM, Fleischer RL, Likes RS: Changes in Subsurface Radon Concentration Associated with Earthquakes. Jr Geophysical res,(1980), 85: 3053-3057 pages.
  • Faul H, Wagner GA: Fission Track Dating, in Dating Techniques for the Archaeologist HN Michael and EK Ralph (eds), Cambridge: MIT Press, (1971), 152- 156 pages.
  • Macdougall JM: Meteoritics,(1975), 10:449 pages.
  • Bodu R, Bouzigues H, Morin N, Pfiffelman JP: On the Existence of Amomalous Isotopic Abundances in Uranium from Gabon. Compt rend Paris, (1972), 275:1731-1732 pages.
  • Hansen P, Heitmann H, Smit PH: Nuclear Tracks in Iron Granet Films. Phys Rev, (1982), B26:3539 pages.
  • Khan HA, Brandt R, Hirdes D, Tress G, Dersch G, Jamil K: Use of Mica Nuclear Filter in the development of a Background Free Radon Presonnel Dosimeter. Journal of Aerosol Science, (1983), 14:232-237 pages.
  • Poulsen H. P., Neuefeind J., Neumann H. B., Schneider J. R., Zeidler M. D., Amorphous silica studied by high energy X-ray diffraction, Journal of non- crystalline solids 188(1,2), (1995), 63-74 pages.
  • Martin, B.R.; Shaw G.; Particle Physics 3 rd Edition ISBN 978-0-470-03293-0.(cloth),ISBN 978-0-470-03294-7(Pbk.),(2008).
  • Heuser J.M.; Ivanov V.V., The Compressed Baryonic Matter experiment at FAIR: physics of strangeness and charm, status of preparations, In Journal of Physics G Nuclear and Particle
There are 20 citations in total.

Details

Primary Language English
Journal Section Research Papers
Authors

Oğuzhan Dervişağaoğlu 0000-0003-3901-9238

Project Number ----------
Publication Date June 30, 2020
Submission Date March 14, 2020
Acceptance Date April 2, 2020
Published in Issue Year 2020 Volume: 3 Issue: 1

Cite

APA Dervişağaoğlu, O. (2020). Usage of Obsidian (Igneous Energy) in Both Radiation Detection and Fixed-Target Machine in Discovery of Subatomic Particles. Journal of Investigations on Engineering and Technology, 3(1), 6-9.